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Methane Hydrate Formation and Dissociation in the Presence of Silica Sand and Bentonite Clay

机译:硅砂和膨润土存在下甲烷水合物的形成与离解

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摘要

The formation and dissociation of methane hydrates in a porous media containing silica sand of different sizes and bentonite clay were studied in the presence of synthetic seawater with 3.55 wt% salinity. The phase equilibrium of methane hydrate under different experimental conditions was investigated. The effects of the particle size of silica sand as well as a mixture of bentonite clay and silica sand on methane hydrate formation and its dissociation were studied. The kinetics of hydrate formation was studied under different subcooling conditions to observe its effects on the induction time of hydrate formation. The amount of methane gas encapsulated in hydrate was computed using a real gas equation. The Clausius-Clapeyron equation is used to estimate the enthalpy of hydrate dissociation with measured phase equilibrium data.
机译:在含3.55 wt%盐度的合成海水存在下,研究了甲烷水合物在多孔介质中的形成和分解,该介质包含不同尺寸的硅砂和膨润土。研究了不同实验条件下甲烷水合物的相平衡。研究了硅砂的粒径以及膨润土和硅砂的混合物对甲烷水合物形成及其离解的影响。在不同的过冷条件下研究了水合物形成的动力学,观察了其对水合物形成诱导时间的影响。使用实际气体方程式计算包裹在水合物中的甲烷气体的量。 Clausius-Clapeyron方程用于根据测得的相平衡数据估算水合物离解的焓。

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